Seismic activity in active volcanic environment consists of many different kind of signals. Volcano-tectonic earthquakes (VT), low frequency earthquakes (or long period, LP), explosion quakes and volcanic tremor are the most common endogenous sources (McNutt, 2005; Chouet, 2003). Landslides and rockfalls are frequently observed on steep volcanoes and caldera walls, due to slope failures.
SEISMIC MONITORING OF MT. VESUVIUS BY ARRAY METHODS
LA ROCCA, MARIO;
2012-01-01
Abstract
Seismic activity in active volcanic environment consists of many different kind of signals. Volcano-tectonic earthquakes (VT), low frequency earthquakes (or long period, LP), explosion quakes and volcanic tremor are the most common endogenous sources (McNutt, 2005; Chouet, 2003). Landslides and rockfalls are frequently observed on steep volcanoes and caldera walls, due to slope failures.File in questo prodotto:
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